Sea surface temperature increase in the global ocean exhibits marked spatial and temporal variations, with warming in the North Pacific significantly higher than in other basins since 2013. This accelerated warming is related to a shoaling of ocean surface mixed-layer depth and is partially dampened by an increase in anomalous net surface heat flux from the ocean. Among heat-flux components, latent heat flux is dominant.

中文翻译：

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2013年以来北太平洋加速变暖

全球海洋海面温度升高表现出明显的时空变化，2013年以来，北太平洋变暖幅度明显高于其他盆地。这种加速变暖与海洋表面混合层深度变浅有关，并受到以下因素的部分抑制：来自海洋的异常净表面热通量增加。在热通量成分中，潜热通量占主导地位。